Note that ppm and delta13C are not the same at all altitudes and evolve progressively, as illustrated by the airborne measurements of Nakazawa et al., Time and space variations of
the carbon isotopic ratio, Tellus, 1993.
In other words, if all of the terrestrial carbon today (in forests, animals, soils, etc.) were converted to carbon dioxide and returned to the global inorganic carbon pool, the change in the global
carbon isotopic ratio would only be a third as big as that observed during the PETM!
In collaboration with the Institute for Arctic and Alpine Research (INSTAAR) of the University of Colorado, ESRL / GMD now routinely monitors
carbon isotopic ratios of CO2 and CH4.
Not exact matches
By comparing the
isotopic ratios of nitrogen and
carbon in the lions» remains with that of contemporary lions, humans and herbivore prey, Justin Yeakel of the University of California, Santa Cruz, estimates the lions ate around 35 people.
By comparing the
isotopic ratios of nitrogen and
carbon in the lions» remains with that of contemporary lions, humans and herbivore...
As a result, methane emissions have distinct
isotopic values: Methane emitted from any microbially driven source such as wetlands or agriculture have values of about -60 ‰ (signifying a relatively low
ratio of
carbon - 13 to
carbon - 12); oil, gas, and coal emissions have an average
carbon isotopic value of -37 ‰; and tree and crop burning averages about -22 ‰.
Animals that live in the sea have
ratios of
carbon and nitrogen isotopes that differ from those found in terrestrial animals, and this
isotopic signature is passed on to the people who eat them.
Because the
isotopic ratios of
carbon and hydrogen display geographic variation, the composition of a feather can reveal where the bird was when the feather grew.
One of Mojzsis's former coauthors, geochemist Gustaf Arrhenius of the Scripps Institution of Oceanography, showed how the Isua
carbon -
isotopic ratio could arise by geologic activity alone, if certain iron minerals in the rock were melted and pressed together over time.
The information about oxygen concentration comes from the
isotopic composition of
carbon or rather from the
ratio between the stable
carbon isotopes 12C and 13C.
Initial SAM results show an increase of 5 percent in heavier isotopes of
carbon in the atmospheric
carbon dioxide compared to estimates of the
isotopic ratios present when Mars formed.
Next, the methane in this air is combusted to produce
carbon dioxide, which is analysed for its
carbon isotopic composition — or
carbon - 13 to
carbon - 12
ratio.
Its
isotopic signature is depleted in the
carbon - 13 isotope, which explains why the atmospheric
ratio of
carbon - 12 to
carbon - 13 has been going down as anthropogenic
carbon dioxide goes up.
«THE stable
carbon isotopic (13C / 12C) record of twentieth - century tree rings has been examined1 - 3 for evidence of the effects of the input of isotopically lighter fossil fuel CO2 (δ 13C ~ -25 ‰ relative to the primary PDB standard4), since the onset of major fossil fuel combustion during the mid-nineteenth century, on the 13C / 12C
ratio of atmospheric CO2 (δ 13C ~ -7 ‰), which is assimilated by trees by photosynthesis.
Curiously, the PETM was accompanied by an exceptionally large change to the global
carbon cycle as indicated by a large drop in the
isotopic ratio of 13C to 12C in the ocean and on land.
If he wanted to apply his scientific credentials to a scientific matter in climate, he might turn to what the
isotopic ratio of
carbon (13C / 12C) needs to be in atmospheric CO2 concentration to constitute a fingerprint of human origin.
«Measurement of atmospheric mixing
ratios, decline of O2 mixing
ratios, pCO2 in the ocean, and the
isotopic carbon composition and other stuff tells us about the source of CO2 increases.
Which is ludicrous in the context of CO2, since we can measure
isotopic ratio changes (indicating the change in old
carbon versus fresh
carbon) and have good accounting for human inputs to the system versus sources and sinks.
Looking at the
isotopic record from the PETM, scientists see both
carbon and oxygen isotope
ratios spiking in exactly the way we expect to see in the Anthropocene record.
The researchers were able to discern agricultural methane from other sources of methane by looking at the gas»
isotopic signatures — or the
ratio of various
carbon isotopes — using data from atmospheric monitoring stations around the world.